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Neogenní a kvartérní sedimenty v oblasti Nového Hrádku (západní část NP Podyjí)
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SYSNO ASEP 0522237 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve SCOPUS Title Neogenní a kvartérní sedimenty v oblasti Nového Hrádku (západní část NP Podyjí) Title Neogene and Quaternary deposits in the closest surroundings of the Nový Hrádek (the Podyjí National Park) Author(s) Nehyba, S. (CZ)
Kirchner, Karel (UGN-S) RID, ORCID
Kuda, František (UGN-S) RID, ORCIDNumber of authors 3 Source Title Geologické výzkumy na Moravě a ve Slezsku. - : Masarykova univerzita - ISSN 1212-6209
Roč. 26, 1-2 (2019), s. 49-57Number of pages 9 s. Publication form Online - E Language cze - Czech Country CZ - Czech Republic Keywords Lower Miocene ; Quaternary ; provenance analysis ; depositional environment Subject RIV DB - Geology ; Mineralogy OECD category Geology Method of publishing Open access Institutional support UGN-S - RVO:68145535 EID SCOPUS 85079221579 DOI 10.5817/GVMS2019-1-2-49 Annotation Neogene deposits of the Carpathian Foredeep were newly recognized in the sedimentary succession within the outcrop close to Nový Hradek site in the area of the Podyjí National Park covered by extensive Quaternary deposits. Facies analysis shows that the recognised Neogene beds represent fluvial deposits. Two facies associations were identified within the Quaternary deposits. Although both of them are interpreted as colluvial deposits, they were formed by a series of gravity flows with highly varied water content. Comparison of Neogene and Quaternary deposits in the surroundings of Nový Hrádek and occurrences of similar sediments within the National Park Thayatal in Austria (e.g. surroundings of Merkersdorf) might provide a further data about the poorly known history of the area during Neogene. Description in English Neogene deposits of the Carpathian Foredeep were newly recognized in the sedimentary succession within the outcrop close to Nový Hradek site in the area of the Podyjí National Park covered by extensive Quaternary deposits. Facies analysis shows that the recognised Neogene beds represent fluvial deposits. Two facies associations were identified within the Quaternary deposits. Although both of them are interpreted as colluvial deposits, they were formed by a series of gravity flows with highly varied water content. Comparison of Neogene and Quaternary deposits in the surroundings of Nový Hrádek and occurrences of similar sediments within the National Park Thayatal in Austria (e.g. surroundings of Merkersdorf) might provide a further data about the poorly known history of the area during Neogene. Workplace Institute of Geonics Contact Lucie Gurková, lucie.gurkova@ugn.cas.cz, Tel.: 596 979 354 Year of Publishing 2020 Electronic address https://journals.muni.cz/gvms/article/view/11832
Number of the records: 1